Pangolin Diamonds Corp. announced update on recent activities at its various projects in the Republic of Botswana, Africa. Highlights Include: Positive drill results at Kweneng, 52.5% of chromites recovered from soils at Kweneng indicative of diamond stability field, 68 aeromagnetic targets identified at Motloutse and Malatswae. Kweneng: Drilling intersected a shallow (< 1 m overburden) phlogopite and clinopyroxene rich ultramafic hypabyssal dyke of approximately 6m in true width. Processing of 25 kg drill chips through Pangolin's in-house 1 TPH DMS plant produced chromite, clinopyroxenes, and what is interpreted as fragments of a chromite-garnet peridotite. The Kweneng Project is located about 20 km north of Botswana's capital, Gaborone. The dyke material is highly altered and is currently interpreted as a phlogopite-rich lamprophyre - similar to the diamondiferous lamprophyres discovered by Southern Africa Minerals Corporation in 1998 approximately 33 km to the north. Pangolin's samples will be submitted for petrographic identification. This discovery came on the back of an extensive soil sampling program that identified a chromite anomaly measuring approximately 850 m x 250 m. Based on the indicator distribution and the relative location of the dyke, it is expected that more dykes may be present in the area. A soil sampling programme will continue once the lockdown is lifted to determine the horizontal extent of the dyke, locating any diatreme structures associated with the dyke as well as locating additional dykes within the KW04 area. Dykes have been mined in South Africa for diamonds to depths exceeding 1,000 metres below the surface. Significant diamonds mines have been established on the Bellsbank, Bobbejaan, Ardo, Helam, Roberts Victor, Star and Klipspringer dykes. Economic kimberlite dykes normally average 60 cm - 80 cm in width and tend to maintain their width and grade with increasing depth. Chromites have been identified as diamond inclusions in West Africa, Dokolwayo in Swaziland, the five mines in Kimberley, Roberts Victor Star (all in South Africa), the Diavik kimberlite in Canada and Murowa as well as River Ranch in Zimbabwe. A total of 326 kimberlite indicator minerals from surface soil samples (KIMs) were submitted to C.F. Mineral Research. 52.5% of chromites analyzed were classified as being derived from a "diamond friendly" environment in the mantle: 23% classified as CR DI; Chromite with major element diamond-inclusion composition, and 29.5% classified as CR DI; Diamond-Inclusion Chromite from favorable harzburgite source. Chromites with Cr2O3 in excess of the stoichiometric limit of 67.9% Cr2O3 comprised 5.5 % of the population, thus indicating a derivation from a highly oxygen reduced environment which is favorable for the formation of diamonds. Subsequent to this publication, chromites have been identified as diamond inclusions in the Diavik kimberlite in Canada and Murowa and River Ranch in Zimbabwe.